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Book Chapter

Geology of the Trenton Limestone in Northwestern Ohio

By
Lawrence H. Wickstrom
Lawrence H. Wickstrom
Ohio Department of Natural Resources Division of Geological Survey Columbus, Ohio
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John D. Gray
John D. Gray
New York State Electric & Gas Corporation East Binghamton, New York
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Published:
January 01, 1988

Abstract

The Trenton Limestone of northwestern Ohio consists of three primary facies: open shelf, platform margin, and platform. The platform margin and platform facies appear to be equivalent to the Point Pleasant Formation. Secondary dolomitization of the Trenton Limestone has resulted in a number of zones and types of dolomite within the unit. A combination of dolomitization models involving shale dewatering and fluid migration along fracture trends are presented to explain the dolomite occurrence.

A thorough understanding of Trenton lithologies, depositional and tectonic settings, and diagenesis should aid future exploration efforts within this once prolific producer of northwestern Ohio.

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Contents

AAPG Studies in Geology

The Trenton Group (Upper Ordovician Series) of Eastern North America: Deposition, Diagenesis, and Petroleum

Brain D. Keith
Brain D. Keith
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American Association of Petroleum Geologists
Volume
29
ISBN electronic:
9781629811352
Publication date:
January 01, 1988

GeoRef

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